TABLE 23
Mean Thermodynamic Values for Europe
z
T
P
p
CP
Q
9
i
9
Si — So
Wi-
Wo
Ui-U
Ki o
20000
19000
18000
17000
219.5
9141
0.2220
657.15
0.8
-3231
-14.747
4658
-7887
16704
16000
223.4
10983
.2476
689.35
2.5
-2791
-12.620
4962
-7753
18497
15000
221.2
12819
.2764
731.44
3.9
-2392
-11.158
5209
-7602
20083
14000
220.3
14972
.3086
769.99
8.6
-1955
- 8.641
5540
-7494
21850
13000
215.7
17017
.3422
799.60
14.3
-1702
- 7.487
5730
-7431
23883
12000
215.8
19942
.3830
836.65
16.4
-1381
- 6.326
5948
-7329
26548
11000
218.7
23341
.4283
863.20
17.8
-1190
- 5.345
6096
-7285
29953
10000
226.0
27198
.4780
873.16
19.3
-1089
- 4.722
6164
-7253
34502
9000
232.8
31606
.5315
884.82
20.7
-1131
- 4.768
6248
-7379
40630
8000
241.1
36509
.5890
890.49
18.4
-1034
- 4.229
6302
-7336
45275
7000
249.0
41972
.6504
897.75
16.3
- 920
- 3.647
6329
-7249
51345
6000
256.1
48053
.7162
907.35
12.6
- 793
- 3.083
6405
-7198
57729
5000
262.6
54819
.7865
919.62
14.1
- 650
- 2.578
6511
-7160
64352
4000
268.3
62353
.8620
934.08
13.0
- 530
- 1.957
6601
-7131
71739
3000
274.3
70722
.9429
947.41
12.6
- 380
- 1.375
6717
-7097
77430
2000
279.1
80030
1.0299
964.88
11.8
- 241
- 0.857
6825
-7066
86011
1000
284.8
90345
1.1224
979.50
9.2
- 76
- 0.241
6969
-7045
94582
100
289.4
100419
1.2101
993.58
6.1
meters of the ground, and involving a supply of latent heat by
the condensation of aqueous vapor into water in cloud formation
by (295); (3) that in the cirrus cloud region, 9,000 to 15,000
meters elevation, according to the latitude, due to ice formation
from frozen water or vapor by (296). In this cirrus region there
are other sources of heat supply, such as an accumulation of
heat from absorption of radiation producing the new rate of
loss of free heat per 1,000 meters. Take the differences in the
(Qi — Q 0 ) columns, and the mean values fall into two groups,
omitting those in the cirrus layers.
Europe, 12000 to 17000 A (Qi — Q 0 )
Tropics, 14000 to 17000
Europe, 1000 to 11000 “ =-133
Tropics, 1000 to 13000 “ = — 140
— 370 per 1000 meters.
- 476
